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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/988658.rdf" xlink:actuate="onRequest">Sulfur hexafluoride and helium data from a tracer release experiment conducted in July 2022 in the central Baltic Sea during research cruise EMB295 on the R/V Elisabeth Mann Borgese</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Dobashi, R., Ho, D. T. (2026) Sulfur hexafluoride and helium data from a tracer release experiment conducted in July 2022 in the central Baltic Sea during research cruise EMB295 on the R/V Elisabeth Mann Borgese. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-02-05 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.988658.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>CenBASE ³He and SF₆ data Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;The Central Baltic Air-Sea Exchange Experiment (CenBASE) was conducted from June to July 2022 on board the R/V Elisabeth Mann Borgese (research cruise EMB295), in an area of the central Baltic Sea east of Gotland, Sweden.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;On 6 July 2022, ³He and SF₆ were injected at approximately 7 meters (m) depth in a hexagonal spiral pattern with a diameter of about 1 kilometer (km), centered at 57.263°N, 20.147°E over the course of 40 minutes. After the injection, discrete samples were taken approximately every 12 hours in the water column near the center of the SF₆ patch using a rosette with a conductivity, temperature, and depth (CTD) sonde and 13 5-liter (L) Niskin bottles. 250-milliliter (mL) syringes were used to obtain discrete SF₆ samples from the Niskin bottles. For discrete ³He samples, about 40 mL of seawater were collected in copper tubes placed in aluminum channels. Stainless steel clamps were used to seal the tubes at both ends for later shore-based measurements.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SF₆ concentrations were measured onboard using a purge-and-trap SF₆ analysis system (Bullister and Weiss, 1988; Gerke et al., 2024). This system separated SF₆ from other gases and measured its concentration by a gas chromatograph equipped with an electron capture detector (GC-ECD). Approximately 200 mL of the water sample were injected into a purge-and-trap unit. Nitrogen served as the carrier gas to purge the samples, and the gases were trapped on a 70-centimeter (cm) column filled with Heysep D (60/80 mesh). The trap was maintained at a temperature of approximately −70 degrees Celsius (°C) by suspending it over liquid nitrogen. The trapped analytes were then desorbed by heating the trap to 100°C. Separation was achieved using a 90-cm pre-column filled ⅓ with Porasil C and ⅔ with Molsieve 5A, and a 220-cm main column, packed 90% with Carbograph 1AC and 10% with Molsieve 5A.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The ³He samples were shipped to the laboratory at the Institute of Environmental Physics at the University of Bremen for analysis. In the laboratory, after being removed from the copper tube, the samples were released into glass bulbs. From there, they were transferred into glass ampoules, which were then sealed for analysis with a helium isotope mass spectrometer (MAP 215-50). δ³He precision for ocean samples is usually better than 0.5% (Sültenfuß et al., 2009).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/988111.rdf" xlink:title="OCE-2123997" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2123997 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2123997</gmx:Anchor>
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&lt;p&gt;The process that controls the exchange of gases between the atmosphere and the ocean plays an important role in regulating global climate, since it influences the amount of atmospheric greenhouse gases and aerosol precursors. Once in the atmosphere, these substances influence global and regional climate. Over the past 30 years, significant advances have been made in understanding this process in the open ocean away from the coasts, and how wind speed controls this process. These advances are mainly due to improvements in experimental techniques, and a number of successful scientific experiments in the open ocean. However, it is not clear if the same understanding applies to inland seas like the Baltic Sea. There, the presence of surfactants, which are biological and chemical substances that concentrate at the sea surface, and the lower salinity, could influence how wind affects this process in a different way than in the open ocean. In this project, a team of investigators will conduct an experiment that aims to assess these processes in the Baltic and compare them to previous experiments in the open ocean.&lt;/p&gt;
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	Description: &lt;p&gt;Date and time in UTC in ISO 8601 format&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993898.rdf
	Name: latitude
	Units: decimal degrees
	Description: &lt;p&gt;Latitude of sampling station&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993900.rdf
	Name: longitude
	Units: decimal degrees
	Description: &lt;p&gt;Longitude of sampling station&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993902.rdf
	Name: depth_m
	Units: meters (m)
	Description: &lt;p&gt;Depth&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993904.rdf
	Name: temperature_C
	Units: degrees Celsius (°C)
	Description: &lt;p&gt;Temperature from Niskin bottles&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993905.rdf
	Name: salinity
	Units: PSU
	Description: &lt;p&gt;Salinity from Niskin bottles&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993906.rdf
	Name: He3_excess
	Units: cubic centimeters at standard temperature and pressure per gram times 10^-16 (ccSTP/g*10-16)
	Description: &lt;p&gt;3He excess concentrations calculated from the measured 3He/4He ratio and the 4He concentration&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/993907.rdf
	Name: SF6_pmol_kg
	Units: picomoles per kilogram (pmol/kg)
	Description: &lt;p&gt;Sulfur hexafluoride (SF6) concentration&lt;/p&gt; 
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&amp;lt;p&amp;gt;On 6 July 2022, ³He and SF₆ were injected at approximately 7 meters (m) depth in a hexagonal spiral pattern with a diameter of about 1 kilometer (km), centered at 57.263°N, 20.147°E over the course of 40 minutes. After the injection, discrete samples were taken approximately every 12 hours in the water column near the center of the SF₆ patch using a rosette with a conductivity, temperature, and depth (CTD) sonde and 13 5-liter (L) Niskin bottles. 250-milliliter (mL) syringes were used to obtain discrete SF₆ samples from the Niskin bottles. For discrete ³He samples, about 40 mL of seawater were collected in copper tubes placed in aluminum channels. Stainless steel clamps were used to seal the tubes at both ends for later shore-based measurements.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;SF₆ concentrations were measured onboard using a purge-and-trap SF₆ analysis system (Bullister and Weiss, 1988; Gerke et al., 2024). This system separated SF₆ from other gases and measured its concentration by a gas chromatograph equipped with an electron capture detector (GC-ECD). Approximately 200 mL of the water sample were injected into a purge-and-trap unit. Nitrogen served as the carrier gas to purge the samples, and the gases were trapped on a 70-centimeter (cm) column filled with Heysep D (60/80 mesh). The trap was maintained at a temperature of approximately −70 degrees Celsius (°C) by suspending it over liquid nitrogen. The trapped analytes were then desorbed by heating the trap to 100°C. Separation was achieved using a 90-cm pre-column filled ⅓ with Porasil C and ⅔ with Molsieve 5A, and a 220-cm main column, packed 90% with Carbograph 1AC and 10% with Molsieve 5A.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The ³He samples were shipped to the laboratory at the Institute of Environmental Physics at the University of Bremen for analysis. In the laboratory, after being removed from the copper tube, the samples were released into glass bulbs. From there, they were transferred into glass ampoules, which were then sealed for analysis with a helium isotope mass spectrometer (MAP 215-50). δ³He precision for ocean samples is usually better than 0.5% (Sültenfuß et al., 2009).&amp;lt;/p&amp;gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;where:&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;[⁴He]eq is the atmospheric equilibrium concentration of ⁴He (Weiss, 1971);&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;Ra is the ³He/⁴He ratio in the atmosphere (1.386 × 10^&amp;lt;sup&amp;gt;-6&amp;lt;/sup&amp;gt; (Clarke et al. 1976));&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;From&amp;lt;em&amp;gt; (1 - a&amp;lt;/em&amp;gt;), a is the solubility isotope effect (0.983 (Benson and Krause, 1980)).&amp;lt;/p&amp;gt;</gco:CharacterString>
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- Converted the date-time column to ISO 8601 format.
- Renamed fields to comply with BCO-DMO naming conventions.
- Saved the final file as &amp;quot;988658_v1_cenbase_3he_sf6.csv&amp;quot;.</gco:CharacterString>
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